2019
DOI: 10.4095/321379
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Abstract: The 2019 field work on Prohibition Creek (SE of Norman Wells), a joint effort of GSC-Calgary and the DEEP research group of the University of Liverpool (UK), aimed to remeasure and sample the Eifelian-Frasnian succession of the Hume Formation and the Horn River Group. The latter is well exposed along Prohibition Creek and recommended as a reference section for the 'Canol shale play' in the adjacent Mackenzie Valley as rocks in studied outcrops occur in the zone of relatively low thermal maturity with high poss… Show more

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“…The upper 61 m of the Hume Formation at Prohibition Creek mainly consist of bioclastic mudstone and wackestone with birds-eye fenestral structures and rare macrofossils, and wackestone/packstone in the uppermost 3 m and lowermost 10 m of the studied interval (Kabanov et al, 2019). Most archival and recent samples taken for conodont biostratigraphy in this part of the Hume were barren, except for a few samples in the wackestone/packstone beds.…”
Section: Age Constraintsmentioning
confidence: 97%
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“…The upper 61 m of the Hume Formation at Prohibition Creek mainly consist of bioclastic mudstone and wackestone with birds-eye fenestral structures and rare macrofossils, and wackestone/packstone in the uppermost 3 m and lowermost 10 m of the studied interval (Kabanov et al, 2019). Most archival and recent samples taken for conodont biostratigraphy in this part of the Hume were barren, except for a few samples in the wackestone/packstone beds.…”
Section: Age Constraintsmentioning
confidence: 97%
“…We assessed the Middle Devonian limestones of the Hume Formation and the basinal mudrocks of the Middle Devonian Hare Indian and Frasnian Canol Formations (Kabanov, in press). For an extended description of these units in Prohibition Creek, see Kabanov et al (2019). Our initial aim was to capture the full section, but the Hare Indian and Canol shales were found too fissile to acquire core plugs.…”
Section: Canadamentioning
confidence: 99%
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